Wednesday, December 7, 2011

Major Storm Opens December 2011


Town of Wise
December 7, 2011
Decorated For The Holiday Season
Photograph by Roddy Addington - © All Rights Reserved.


A fast & furious fall of heavy snow capped off yet another major storm to close the first week of December 2011 and begin meteorological winter.

Elevation 2454 feet
Afternoon of December 7, 2011
Winter Majesty In The Town of Wise
Photograph by Roddy Addington - © All Rights Reserved.

It was a scene of pure beauty in Wise where Holiday decor was perfected by Mother Nature's furious afternoon burst of heavy snow.

December 7, 2011
Winter Wonderland On Wise Plateau
Snow Sticking To Power Lines In Wise Despite Wind
Photograph by Roddy Addington - © All Rights Reserved.

A general 2" to 4" of snow accumulation was reported across the Norton-Wise area during the afternoon.

It should be pointed out that this fast hitting event produced some interesting effects, as despite wind that blasted snow onto poles it still managed to stick to overhead wires amid the quick switch from drenching rain to heavy, wet snow.

December 7, 2011
High Chaparral of High Knob Massif
Heavy Snow, Wind, And Low Clouds
Photograph by Darlene Fields - © All Rights Reserved.

A few air miles south of Wise conditions got BAD amid the High Knob highcountry, with strong N-NW winds and near whiteout conditions above 2700 feet, as well documented by Darlene Fields.

Elevation 3300 feet
High Chaparral of High Knob Massif
WIND Blasted Trees & Snow Covered Roads
Photograph by Darlene Fields - © All Rights Reserved.

Snow was blasted onto trees from bottom to top as roads gradually disappeared beneath the furious fall to create surreal looking scenes amid icy clouds of wind driven flakes.

Afternoon of December 7, 2011
Remnant Massif of the High Knob Landform
Beautiful Mid-Afternoon Darkness In The Highcountry
Photograph by Darlene Fields - © All Rights Reserved.

Observe how snow was drifted up around tree trunks in the above scene, amid an eerie looking afternoon darkness of the deep woods.

December 7, 2011
Lower End Snow Depths In High Chaparral
Photograph by Darlene Fields - © All Rights Reserved.

As heavy snow began to wane it left snow depths that varied from 2" to 3" on the lower end of the measuring stick to as much as 6" on the higher end, with larger drifts.

December 7, 2011
High Chaparral of the High Knob Massif
Half A Foot of Snow Depth On The Ground
Photograph by Darlene Fields - © All Rights Reserved.

On the main summit, above 4000 feet, it was a different story as the sustained winds were so strong that they literally swept highly exposed places nearly bare!

December 7, 2011
Wind Swept Gap Between High Knob & Eagle Knob
Photograph by Roddy Addington - © All Rights Reserved.

That is actually a great stop motion shot by Roddy as upon close inspection one can see large snowflakes that are moving sideways and even UP in direction.  Look in particular along right side of picture as those cotton-like blobs are snowflakes moving UPslope across the lofty summit!

The above is why it is sometimes nearly useless to measure precipitation along these highly exposed convex crestlines that face winds, as precipitation elements ( including rain ) not only move horizontally but also vertically in direction when upslope forcing is strong.

Elevation 4100 feet
Bitter Cold Fury & Low Visibility 
Wind Blasted Along The Crest Zone
Photograph by Roddy Addington - © All Rights Reserved.

Looking from High Knob along the lee side of Forest Service 238 much deeper snow can be seen in the above photo by Roddy taken along the southeast slope of Eagle Knob.

So where does all that snow go?  If one looks around it typically can be found along lee sides of ridges, in drifts, and even in this setting over into the lofty High Knob Lake Basin!

December 7, 2011
Near Summit of High Knob Peak
Wind Sculpturing Around Large Rock On Ground
Photograph by Roddy Addington - © All Rights Reserved.

On small scales one can also see the same type of effects around objects on the ground, like this rock Roddy photographed above with much more snow on one side than the other.

[ Not a truly ideal example above since both sides of this rock were exposed to 30-40+ knot winds, as Roddy well verified and felt in middle 20s air temps that blasted him & the ground. Ouch! ].

Elevation 3300 feet
High Chaparral of High Knob Massif
Snowboard Adjacent To 5-6" Ground Depths
Photograph by Darlene Fields - © All Rights Reserved.

A very good way to measure snow and to determine how much new snow falls once the ground becomes covered is to use snowboards, placed on or above ground in various locations.

The above method being detailed nicely by 
The Snow Booklet of Colorado State University.

Picnic tables, or other types of above ground objects which are not going to be moved during an event, can also make good measuring boards.

December 7, 2011
High Chaparral of High Knob Massif
Outdoor Picnic Table Used As Snowboard
Photograph by Darlene Fields - © All Rights Reserved.

A key feature of this method being to measure and sweep the boards clean once every 6 hours, ideally, that snow is falling ( with four but not more than four measurements during a 24-hour period ).

December 7, 2011
HUGE Flakes In High Chaparral of High Knob Massif
Photograph by Darlene Fields - © All Rights Reserved.

Another notable feature of this event was huge snowflake sizes, especially during intervals where strong winds decreased just a little.


Winter Storm Along 
The Tennessee Valley Divide

December 7, 2011
Heavy Snowfall On Long Ridge At 4:23 PM
Photograph by Genevie Riner - © All Rights Reserved.

My friend Genevie Riner documented the fury of this snowstorm as it engulfed the high ridges along the Tennessee Valley Divide.

December 7, 2011
Heavier Snowfall On Long Ridge At 4:40 PM
Photograph by Genevie Riner - © All Rights Reserved.

Given soaking rains which fell through morning hours it was rather shocking to see how fast snow was able to stick to everything!

Afternoon of December 7, 2011
Rapid Transformation Into Winter - Snowfall & Wind
Photograph by Genevie Riner - © All Rights Reserved.

Accumulations became significant, with an official storm total of 4.6" being measured by Genevie & Wayne Riner at Nora 4 SSE ( elevation 2650 feet ).

December 7, 2011
Snow Piling Up Amid Fury Of Storm At 4:54 PM
Photograph by Genevie Riner - © All Rights Reserved.

Clearing skies into December 8 created simply gorgeous scenes on the high ridges.

December 8, 2011
Long Ridge of Sandy Ridge of the Tennessee Valley Divide
Heaviest Snow Of Early Winter Along The High Ridges
Photograph by Genevie Riner - © All Rights Reserved.

Observe how thick snow has stuck to trees amid folds of the terrain, beneath ridges, while those trees exposed are mostly bare to create striking contrasts in the morning light!

Morning of December 8, 2011
Looking Along The Tennessee Valley Divide
Photograph by Genevie Riner - © All Rights Reserved.

Genevie captured an interesting scene in this next photograph as a rather distinct morning inversion layer had developed, denoted by the sharp cloud line below, with warming temps amid a zone from around 3500 to 6500 feet that trapped moist air near the surface.

Morning of December 8, 2011
Long Ridge of Tennessee Valley Divide
Top Of Inversion Layer - View Toward Pine Mountain
Photograph by Genevie Riner - © All Rights Reserved.

Although morning minimums dipped into bitter mid-upper 10s across much of the snow area lying above 2200 feet in elevation, the presence of upslope cloudiness throughout the night beneath this inversion layer kept temps from getting even colder over the fresh snow cover ( the inversion mixing out over higher terrain after sunrise but still visible in the far distance, mostly beyond Pine Mountain, toward the Kentucky foothills ).

December 8, 2011
Feeding Time In The Highlands - After A Bitter Night
Photograph by Genevie Riner - © All Rights Reserved.

Mountain ridges & plateaus form many nice communities across Dickenson and Wise counties, with elevated farms that plunge off into deep, twisting hollows.

Snow cover always acts to accentuate the terrain, with every wrinkle & fold becoming visible across this amazing landscape of the southern Appalachians!



First Significant
December Precipitation Event
( December 5-7, 2011 )

December 7, 2011
Standing Water Surrounded By Snow
Photograph by Isaiah Addington - © All Rights Reserved.

Isaiah Addington ( Roddy's son ) captured the major aspect of this event by showing standing water from yet another big precipitation maker that generated strong rises on creeks and rivers.

My friend Andrew Greear measured a total of 2.41" at the Norton Water Plant, with around 0.37" of that being in the form of wet snow, boosting the 2011 tally to 73.24" for the City of Norton.

My friends Otis & Nancy Ward had a precipitation total of 2.55" in the Robinson Knob community of the High Knob Massif, boosting 2011 to 78.29" and their 12-month total to 82.12" ( despite substantial missing gage moisture in deep snows last winter ).

River Rises 11.86 Vertical Feet
River Gage Height At Speers Ferry In Scott County

Run-off from much of this precipitation generated another huge rise on the Clinch River with nearly 12 vertical feet of total increase being observed at Speers Ferry in southern Scott County. 

[ Note that a general 0.30" to 0.60"+ of moisture was locked away in snowfall which reduced run-off during this event ].


Wonderland In Lights
Camp Bethel In Wise, Virginia
December 7, 2011

Magic Of The Holiday Season - Camp Bethel In Lights
Photograph by Roddy Addington - © All Rights Reserved.


Roddy took time to capture the holiday season with a drive out to always beautiful Camp Bethel, resting upon 160 acres on the Tennessee Valley Divide of the Wise Plateau.

The lake at Camp Bethel is only 3.5 air miles north of the northern-most base of the High Knob Massif, near Ramsey, and is approximately 6.6 air miles north-northeast of the Dam at Upper Norton Reservoir.

Lake Elevation of 2520 feet
Snow Adds To Holiday Beauty At Camp Bethel
Photograph by Roddy Addington - © All Rights Reserved.

Several inches of snow added to the beauty of this magical scene by the lake at Camp Bethel, with tree bows hanging low under the high density snow.

December 7, 2011
Beautiful Snow At Camp Bethel
Making Kids Jealous In The Tri-Cities
Photograph by Roddy Addington - © All Rights Reserved.

Scenes such as these no doubt make many kidos, and "grown-ups" too, jealous who missed out on significant snow accumulations in the Tri-Cities to Knoxville corridor of the Great Valley.

Camp Bethel in Wise
Sugar Canes & Snow - Dream Come True
Photograph by Roddy Addington - © All Rights Reserved.

With such strong NW-N winds pushing into windward slopes of the High Knob Landform and higher portions of the Tennessee Valley Divide it is no wonder that sticking snow was hard to come by in the Tri-Cities, given such air trajectories add warming & drying to low-levels of the atmosphere.

NASA Visible Satellite Image At 9:31 AM - December 8, 2011
Image Courtesy of the Earth Science Office

Snow on visible imagery tends to show up best over flatter, more open terrain.  The rolling farms of both Russell & Tazewell counties show up better than their higher mountain ridges.

In the High Knob Landform, a narrow stripe of snow is visible along Wallen Ridge to the Buzzard Roost where it abruptly ends in northeast Lee County.  The crestline of Cumberland Gap NHP is faintly visible along the stateline above far western Lee County.

The crestline of Little Stone and Stone mountains is also visible to just past Cave Springs Wilderness Area, with the inverted V-shape of Powell Valley in Wise County being completed by the bulge of the High Knob Massif to the southeast and the capped crestline of its Little Stone Mountain arm toward the northwest.

Some of the white on this image is clouds where gravity waves are visible across northern portions of West Virginia & Virginia. Wavy cloud streets are also seen where cold air flows over the Atlantic.

Note the abrupt cut-off on snow visible in the above image south of northern Scott County where air flow plunges downward off the highcountry of the High Knob Massif.

The southwest extension of snow visible through Russell County is northeast of the downsloped forced shadowing zone leeward of the massif on N to NW air flow trajectories.

NAM Model 850 MB Chart At 7 PM - December 7, 2011
Image Courtesy of NCEP Central Operations

This is illustrated by the above chart where air flow above the boundary layer of Earth tends to run parallel to the black isobars, or lines of equal pressure ( north to south flow in this case ).

At the surface, by contrast, drag of air flowing across the terrain generates friction that forces a cross-isobaric turning of the wind field as illustrated by the NW wind vector arrows.

The result of these two factors was a strong N-NW air flow crossing the High Knob Massif, with general 3" to 6" snow depths along its windward slopes verses little to no sticking snow leeward of the massif on downslope forced drying & warming. 

[ Renewed lifting by the secondary front range along the TN-NC border, with respect to NW air flow, was required to generate enough cooling to deposit snow once again ( leaving much of the Great Valley devoid of snow accumulations ) ].

Beautiful Camp Bethel in Wise
Lollipops & Snow - Could It Get Any Better?
Photograph by Roddy Addington - © All Rights Reserved.

My friend Darlene Fields captured numerous nice scenes as she came down out of the highcountry toward Tacoma, along State Route 706, during December 8.

Along Stone Mountain Road ( State Route 706 )
Winter Beauty Near Stone Mountain Church
Photograph by Darlene Fields - © All Rights Reserved.

Snow stuck best to trees in sheltered places such as high hollows, coves, and lower portions of the mid-elevation zone where wind speeds were not as strong ( as illustrated on Long Ridge ).

Along State Route 706 in Wise County, Virginia
Canadian Hemlock ( Tsuga canadensis ) Bows In Snow
Photograph by Darlene Fields - © All Rights Reserved.

It was a winter wonderland drive along scenic Stone Mountain highway, State Route 706, with thick snow on trees in sheltered places.

December 8, 2011
Winter Wonderland Drive - High Knob Massif
Photograph by Darlene Fields - © All Rights Reserved.

Snow depth decreased into lower elevations, but it looked pretty sticking to trees and bushes against the blue sky of December 8.

December 8, 2011
Lower Elevations Above Tacoma Valley
Photograph by Darlene Fields - © All Rights Reserved.

A little different from half a foot of depth to add more interesting variety to this already amazing mountain landscape!

High Knob Massif during December 7, 2011
Half A Foot Of Ground Depth - High Chaparral
Photograph by Darlene Fields - © All Rights Reserved.

Speaking of which, check out this latest video production by my friend Richard Kretz who highlights many wonderful attributes of 


Southwest Virginia: 
One Of The Last Great Places On Planet Earth!

Produced & Directed by Richard Kretz


A fantastic overview of biodiversity in the Upper Tennessee River Basin of southwestern Virginia.  Thank you my friend!


[ *Note: A link to this video can always be found along the right column of this website under Richard's name and email address ].

Friday, December 2, 2011

Autumn 2011 Ends WET & Cold


Long Ridge of the Tennessee Valley Divide
At The End Of The Rainbow - November 28, 2011
Photograph by Wayne Riner - © All Rights Reserved.


Wayne Riner  Photograph Thoughts...
"It was the evening before the cold weather to come, and the sun came through to show a rainbow with the bare trees.  A white cloud looks down on the end of the day."

November 2011 was yet another wet month across the High Knob Landform, with totals that locally topped 10.00" in wetter sections of the massif and the Cumberland Gap National Historical Park area.

Harold Jerrell measured 9.43" during November in the Silver Leaf community of Lee County located just southeast of Cumberland Gap National Historical Park.


Climate Statistics For
November 2011

( Lower Elevations of Russell Fork Basin )
Clintwood 1 W - Elevation 1560 feet
Average Daily MAX: 58.5 degrees
Average Daily MIN: 32.4 degrees
MEAN: 45.4 degrees
Highest Temperature: 69 degrees
Lowest Temperature: 20 degrees
Total Precipitation: 4.78"
Total Snowfall: 0.1"
2011 Precipitation: 56.81"

( Northern Base of High Knob Massif )
City of Norton - Elevation 2141 feet
Average Daily MAX: 55.3 degrees
Average Daily MIN: 31.3 degrees
MEAN: 43.3 degrees
Highest Temperature: 65 degrees
Lowest Temperature: 17 degrees
Total Precipitation: 8.08"
Total Snowfall: 2.0"
2011 Precipitation: 70.83"

( Along the Tennessee Valley Divide )
Nora 4 SSE - Elevation 2650 feet
Average Daily MAX: 54.2 degrees
Average Daily MIN: 38.1 degrees
MEAN: 46.2 degrees
Highest Temperature: 64 degrees
Lowest Temperature: 23 degrees
Total Precipitation: 5.45"
Total Snowfall: 1.8"
2011 Precipitation: 53.04"

( Northern End of The Cedars )
Jonesville 3.1 WSW - Elevation 1422 feet
Average Daily MAX: 61.1 degrees
Average Daily MIN: 34.3 degrees
MEAN: 47.7 degrees
Highest Temperature: 69 degrees
Lowest Temperature: 18 degrees
Total Precipitation: 6.62"
Total Snowfall: Trace
2011 Precipitation: 53.18"

In the High Knob Massif November temp means varied from upper 40s to lower 50s by day to upper 20s to lower 30s at night.  The November MAX on Eagle Knob reached 58 degrees and the MIN dropped to 17 degrees ( colder amid snow covered mid-upper elevation basins ).

A general 7.00" to 10.00"+ of total precipitation fell across the massif area during November, including 3" to 5" of snow above 3000 feet.

As of early December there have been 12 days with at least 1" of snow depth across N-NE slopes of the High Knob Lake Basin since October 1, 2011 ( above 3400 feet ).

November 30, 2011
Elevation 4189 feet ( at summit )
RIME Coated Trees - Eagle Knob of High Knob Massif
Photograph by Steve Blankenbecler - © All Rights Reserved.

My friend Steve Blankenbecler captured the beauty of gorgeous rime and blue skies as clouds began to dissipate above a cold Eagle Knob summit on November 30 ( PM MAX of 27 degrees ).

November 2011
Measurable Precipitation Days
Robinson Knob of High Knob Massif
Observers: Otis & Nancy Ward
Elevation 3240 feet
( Daily Amounts Ending At 8 AM )

11/04:  1.00"

11/10:  0.05"

11/15:  0.87"
11/16:  1.71"
11/17:  4.04"
11/18:  0.12"
11/19:  0.09"

11/22:  0.26"
11/23:  1.05"

11/28:  0.09"
11/29:  1.00"
11/30:  0.10"

November 15-19 Total: 6.83"

November Total: 10.38"

Total Since September 1: 23.33"

2011 Total: 75.74" ( M )

12-Month Total: 81.94" ( M )
*( December 2010 to November 30, 2011 )

( M ) - Indicates some missing moisture amid winter snowfall and smaller evaporative losses between hand-measurements during the cold season ( 4"-diameter NWS rain gage ).

*Significant rain gage moisture loss occurred in December 2010 when Joe & Darlene Fields measured 55" of snow in nearby High Chaparral ( 65" to 70" fell at highest elevations in the massif ).

Precipitation received during 2011 and the past several years amid the High Knob Landform has produced a huge precipitation gradient across Virginia that exemplifies differences observed over a much longer period of time, such as the distinct variations recognized in the 1930s and 1940s by Dr. Emma Lucy Braun.


Emma Lucy Braun...
"The Mixed Mesophytic association reaches its best development in the Cumberland Mountains.  There it is most luxuriant in aspect and contains a larger number of species than elsewhere.  There it displays the greatest variety of types, of association-segregates formed by local shifts in dominance of constituent species...when we look beyond the boundaries of this region in any direction, we find mixed mesophytic communities much more circumscribed, much more restricted to particular local environments, and generally containing fewer species or even lacking characteristic species."

Cumberland Mountains
Cumberland Mountain Overthrust Block
Stone Mountain of the High Knob Massif
Eagle Knob Communications Area - November 30, 2011
Image by Steve Blankenbecler - © All Rights Reserved.

*Emma Lucy Braun...
"The Cumberland Mountains section of the Mixed Mesophytic Forest region is essentially coextensive with the physiographic section by the same name.  This is a mountainous section, whose highest and most characteristic part is carved from a large fault block with more or less upturned edges forming the monoclinal bordering mountains - Pine Mountain along the northwest and Cumberland Mountain and Stone Mountain on the southeast."


Although it has been a long time since Lucy Braun and her sister Annette walked the forests of the Cumberlands, her legacy lives on as a pioneer in forest ecology and the first scientist to ever define the extent of this ancient forest.

Emma Lucy Braun...
"The southeastern boundary of the Cumberland Mountains, formed by the escarpment which here is Cumberland and Stone Mountains, is the approximate limit of the area where mixed mesophytic forest prevails."


Lucy Braun is referring to the southeastern extent of what she considered to be the heart and core of the mixed mesophytic forest region, east and southeast of which it becomes relegated only to the best and most mesic sites of localized areas.

The Cumberland Front Along & Northwest of RED Line
Adapted From High Resolution NASA Visible Image

As the High Knob Massif bulges upward into the atmosphere so do precipitation amounts, with a general 70" to 80" in 2011 from the City of Norton across its wide highcountry being in contrast to 53.18" near The Cedars of its calcareous core ( denoted by SW-NE dark green strip above ) to the southwest, 53.04" on Long Ridge of the Tennessee Valley Divide to its northeast, and 43.58" in the Tri-Cities of the Great Valley toward the southeast.

The Cumberland Front, or escarpment, that is referred to by Lucy Braun is formed by the distinct northwestern mountain flank of the High Knob Landform and southeastern base of its remnant massif ( along and northwest of the red line ).

As my research is showing for ALL to see, this marks not only a physiographic boundary but also a distinct climatic boundary that drives all features of this amazingly complex natural world found within the High Knob Landform and its Upper Tennessee & Upper Cumberland basins.


Climate Statistics
For Autumn 2011
( September-November )

November 27, 2011
Long Ridge of Sandy Ridge
Gorgeous Mountain Waves At Sunrise
Photograph by Wayne Riner - © All Rights Reserved.

( Lower Elevations of Russell Fork Basin )
Clintwood 1 W - Elevation 1560 feet
Average Daily MAX: 65.6 degrees
Average Daily MIN: 41.8 degrees
Autumn MEAN: 53.7 degrees
Total Precipitation: 15.58"
Total Snowfall: 0.1"

( Northern Base of High Knob Massif )
City of Norton - Elevation 2141 feet
Average Daily MAX: 63.3 degrees
Average Daily MIN: 40.0 degrees
Autumn MEAN: 51.6 degrees
Total Precipitation: 22.33"
Total Snowfall: 2.3"

( Along the Tennessee Valley Divide )
Nora 4 SSE - Elevation 2650 feet
Average Daily MAX: 62.5 degrees
Average Daily MIN: 45.8 degrees
Autumn MEAN: 54.2 degrees
Total Precipitation: 16.38"
Total Snowfall: 2.2"

( Northern Edge of The Cedars )
Jonesville 3.1 WSW - Elevation 1422 feet
Average Daily MAX: 68.7 degrees
Average Daily MIN: 43.4 degrees
Autumn MEAN: 56.0 degrees
Total Precipitation: 16.84"
Total Snowfall: Trace

In the High Knob Massif temperature means during autumn varied from mid-upper 50s by day amid highest elevations to upper 30s-lower 40s at night.

A general 20.00" to 25.00" of total precipitation fell during the three month period, including 4" to 10" of snowfall above 3000 feet.  This pushed 2011 into the 70-80" range for total precipitation.


November & 2011 Precip Totals
From Virginia And District of Columbia
*( 2011 Totals from January 1 to November 30 )

Lynchburg
November Precipitation: 3.27"
2011 Total: 34.37"

Wallops Island
November Precipitation: 1.98"
2011 Total: 35.11"

Pulaski 2 E
November Precipitation: 3.39"
2011 Total: 35.84"

Gathright Dam
November Precipitation: 3.10"
2011 Total: 36.44"

Danville
November Precipitation: 4.98"
2011 Total: 36.82"

Kerrs Creek 6 WNW
November Precipitation: 3.12"
2011 Total: 37.41"

Covington FP
November Precipitation: 3.10"
2011 Total: 37.49"
( 1 missing day in August )

Wytheville 1 S
November Precipitation: 3.71"
2011 Total: 37.73"
( 1 missing day in August )

Emporia 1 WNW
November Precipitation: 3.53"
2011 Total: 37.87"
( 2 missing days in June )

Lexington
November Precipitation: 4.05"
2011 Total: 38.02"
( 2 missing days in August )

Virginia Beach 2.4 N
November Precipitation: 1.86"
2011 Total: 38.19"
( 2 missing days in May / 1 day in July )

Martinsville FP
November Precipitation: 5.50"
2011 Total: 38.31"

Appomattox
November Precipitation: 3.51"
2011 Total: 38.80"
( 7 missing day during year )

Chase City
November Precipitation: 3.60"
2011 Total: 39.31"
( 2 missing days in August )

Blacksburg
November Precipitation: 3.70"
2011 Total: 40.06"

Bluefield ( West Virginia )
November Precipitation: 3.43"
2011 Total: 40.06"

Woodstock 2 NE
November Precipitation: 3.01"
2011 Total: 40.10"
( 6 missing days during year )

Philpott Dam 2
November Precipitation: 5.35"
2011 Total: 40.82"
( 5 missing days in January-February )

Roanoke
November Precipitation: 4.30"
2011 Total: 40.84"

Staunton WTP
November Precipitation: 2.43"
2011 Total: 41.57"

Bland
November Precipitation: 4.22"
2011 Total: 41.59"
( 3 missing days in January )

Radford 3 N
November Precipitation: 3.54"
2011 Total: 41.70"

Washington Dulles Airport
November Precipitation: 2.18"
2011 Total: 41.74"

Washington National Airport
November Precipitation: 1.94"
2011 Total: 41.99"

Saltville 1 N
November Precipitation: 4.15"
2011 Total: 42.01"

Christiansburg
November Precipitation: 3.76"
2011 Total: 42.63"

Dale Enterprise
November Precipitation: 2.47"
2011 Total: 42.94"
( 1 missing day in February )

Buckingham
November Precipitation: 3.87"
2011 Total: 43.34"
( 1 missing day in August )

Luray 5 E
November Precipitation: 1.79"
2011 Total: 43.77"
( 1 missing day in November )

Waynesboro WTP
November Precipitation: 3.59"
2011 Total: 43.87"
( 2 missing days in March & August )

Charlottesville
November Precipitation: 3.14"
2011 Total: 43.95"

Millgap 2 NNW
November Precipitation: 3.93"
2011 Total: 44.76"

Richmond
November Precipitation: 4.18"
2011 Total: 45.51"

Trout Dale 3 SSE
November Precipitation: 3.73"
2011 Total: 45.91"
( 1 missing day in August )

Richlands
November Precipitation: 4.67"
2011 Total: 46.07"

Burkes Garden
November Precipitation: 4.64"
2011 Total: 46.22"
( 1 missing day in August )

Holcomb Rock
November Precipitation: 4.44"
2011 Total: 46.89"
( 2 missing days in August )

Glasgow 1 SE
November Precipitation: 4.36"
2011 Total: 47.27"
( 2 missing days in August )

Hot Springs
November Precipitation: 5.06"
2011 Total: 47.38"
( 1 missing day in January )

Lebanon
November Precipitation: 4.34"
2011 Total: 48.42"
( 3 missing days in November )

Grundy
November Precipitation: 4.07"
2011 Total: 48.79"

Galax WTP
November Precipitation: 4.54"
2011 Total: 48.84"
( 1 missing day in August )

Norfolk
November Precipitation: 1.84"
2011 Total: 49.54"

Woolwine
November Precipitation: 5.45"
2011 Total: 50.66"
( 1 missing day in August )

Nora 4 SSE
November Precipitation: 5.45"
2011 Total: 53.04"

Jonesville 3.1 WSW
November Precipitation: 6.62"
2011 Total: 53.18"

Clintwood 1 W
November Precipitation: 4.78"
2011 Total: 56.81"

Meadows of Dan 5 SW
November Precipitation: 7.70"
2011 Total: 59.24"

Appalachia Lake Water Plant
November Precipitation: 7.50"
2011 Total: 62.41"

Coeburn Filter Plant
November Precipitation: 6.24"
2011 Total: 62.96"

Big Stone Gap Water Plant
November Precipitation: 7.82"
2011 Total: 65.85"

( Cumberland Gap NHP )
Yellow Creek, KY RAWS
November Precipitation: 7.02"
2011 Total: 67.46"

Norton Water Plant
November Precipitation: 8.08"
2011 Total: 70.83"

Big Cherry Dam of High Knob Massif
November Precipitation: 8.67"
2011 Total: 73.63" ( M )

Robinson Knob of High Knob Massif
November Precipitation: 10.38"
2011 Total: 75.74" ( M )

( M ) - Denotes that total precipitation was greater than rain gage total due to evaporation between hand-measurements and physical gauge losses in deep falls of snow.

( * ) - Days denoted as missing may or may not have had any measurable precipitation at the indicated sites.  All station data should be considered as preliminary until officially checked and accepted by the National Climatic Data Center.


While obvious to anyone looking at the above data, 20" to 40"+ spreads in amounts are no less than HUGE for an 11 month period.

Most important, however, is that in the mean such variations are common as I have documented for many years ( look for final totals when December 2011 ends ).



Wetness Continues To
Rewrite Virginia Climatology

For the past 37-months my featured site has been amid majestic Big Cherry Basin of the High Knob Massif, where hand-measurements by my friend Gary Hampton & Staff of the beautiful, historic town of Big Stone Gap are helping rewrite the known climatology of Virginia.



Big Cherry Dam of High Knob Massif
Monthly Precipitation Totals
Observers: Gary Hampton & Staff
Elevation 3120 feet

2008
November:  4.36"
December: 8.49"

2009
January: 9.23"
February: 4.36"
March: 5.51"
April: 5.40"
May: 7.07"
June: 5.44"
July: 8.42"
August: 7.08"
September: 9.09"
October: 4.36"
November: 3.88"
*December: 11.50"

2010
*January: 6.25"
*February: 4.25"
*March: 4.50"
April: 3.78"
May: 6.99"
June: 9.53"
July: 4.27"
August: 8.91"
September: 2.88"
October: 2.84"
November: 4.05"
*December: 7.35"

2011
January: 4.51"
February: 4.53"
March: 9.85"
April: 10.08"
May: 5.38"
June: 6.16"
July: 7.18"
August: 4.94"
September: 7.28"
October: 5.05"
November: 8.67"

2011 Total: 73.63" ( M )

Orographic Forcing Season Total
November 2010-April 2011: 40.37" ( M )
( 6.06" per month average )

12-Month Total: 80.98" ( M )

24-Month Total: 150.73" ( M )

37-Month Total: 233.42" ( M )

37-Month Mean Monthly Precip: 6.31"

Mean Per 12-Month Periods: 75.72" ( M )

( * ) - Indicates that total was estimated or partly estimated due to severe winter conditions.

( M ) - Denotes that total precipitation was greater than rain gage total due to evaporation between hand-measurements observed at the Dam ( the mean evaporative loss is estimated to have been 3.00" to 3.50" per year as partly based upon observed losses at Clintwood 1 W ) and deep falls of snow greater than the rain gage could physically hold.

[ All measurements courtesy of Superintendent Gary Hampton & Staff at the Big Stone Gap Water Plant in South Fork Gorge ].

While the 6.31" mean monthly precipitation observed during the past 37 months is the highest ever documented in the Old Dominion over such an extended period of time, it is known to be less than what actually fell at Big Cherry Dam.

Conservative estimates for the actual rain gage catch at Big Cherry Dam yield around 6.56" per month when allowing for amounts lost due to evaporation between hand-measurements and winter falls of snow too deep for the rain gage to physically hold.

If all partial estimates & estimates on the 5 months with missing data due to severe winter conditions are taken away the mean monthly precipitation average on the raw rain gauge catch still yields 6.25" ( also the highest on record in Virginia ).

So it is very safe to state as fact that for more than three consecutive years wetter portions of the sprawling High Knob Massif have averaged 75" to 80" of total precipitation, which has never before been documented in Virginia outside of the massif.

Recent 3-year time periods with similar amounts in the High Knob Massif include:

1989-1991
1994-1996
2002-2004

Some of the wettest years of the past 4 decades likely occurred during the active 1970s before any precipitation record keeping began in the City of Norton and High Knob Massif area.  



In The Lifting Zone
Of The High Knob Massif
City of Norton

My friends Tommy Roberts & staff have been helping rewrite Virginia climatology for decades, with data scans through the Climatology Office in Charlottesville, of all available sites, finding the City of Norton to be the wettest location in the state during the 1983-2004 period scanned.

I knew, of course, that the High Knob Massif was wetter since I had been doing surveys of its precipitation since the 1980s on snowfall and 1990s on rain & snow.

The above being a most significant discovery given that the Norton Water Plant had substantial moisture losses in larger falls of snow during the entire 1983-1998 period of its record, when deeper snows could not be held by a 4"-diameter rain gage ( I installed an official 8"-diameter NWS gauge in summer 1998 ).


City of Norton Water Plant
Monthly Precipitation Totals
Observers: Water Plant Staff
Elevation: 2342 feet

2008
November: 3.68"
December: 8.58"

2009
January: 7.34"  
February: 3.27"
March: 5.24"
April: 5.13"
May: 9.72"
June: 7.95"
July: 5.46"
August: 5.19"
September: 6.08"
October: 3.46"
November: 2.77"
December: 7.54"

2010
January: 4.63"
February: 3.37"
March: 3.65"
April: 3.12"
May: 8.60"
June: 5.68"
July: 2.43"
August: 7.65"
September: 3.58"
October: 3.26"
November: 3.67"
December: 6.00"

2011
January: 2.99"
February: 2.96"
March: 8.38"
April: 8.66"
May: 5.13"
June: 6.40"
July: 8.43"
August: 5.55"
September: 9.21"
October: 5.04"
November: 8.08"

2011 Total: 70.83"

Nov 2010-April 2011 Total: 32.66"
Orographic Forcing Season
( 5.44" per month average )

12-Month Total: 76.83"

24-Month Total: 134.01"

37-Month Total: 207.88" 

37-Month Mean Monthly Precip: 5.62"

Mean Per 12-Month Periods: 67.44"

Measuring like clock work every day, with no missing data, the 37-month mean of 5.62" yields 8.28" less precipitation per year than obtained at Big Cherry Dam.

The 2011 period being closest between Big Cherry Dam and the City of Norton, with larger differences observed during the 2009-10 measurement period.  The main point; however, being that actual amounts at Big Cherry Dam were greater than rain gage numbers such that the 37-month difference between the two sites was larger than indicated by these data sets on primary precip.

Addition of secondary moisture sources, such as fog drip from trees and rime deposition on trees, which are not collected by rain gages, makes the Big Cherry Basin much wetter than the Norton Valley over the longer term.

In reality, of course, City of Norton mean monthly precipitation during the past 37-months would have likely produced around 11.00" less per year than Big Cherry Dam had it been possible to also measure every day by hand at the Dam.

Implications of the above are vast, 
and extend over a much longer period of time.


High Knob Landform Forced
Differences Across The Clinch River Basin

Time Period of 1990 to 2003
Annual Precip Variations Between Norton & Lebanon
Wayne Browning Graphic - © All Rights Reserved.

14-Year Annual Mean ( 1990-2003 )

Elevation: 2342 feet at Water Plant
City of Norton: 58.54"

Elevation: 1912 feet
Town of Lebanon: 42.96"
( -15.58" less per year in Lebanon )

Although I have already pointed out that the High Knob Landform and its remnant massif works to force annual precipitation decreases in traveling up stream in the ecologically rich Clinch River Basin, the above graphic illustrates this nicely during a direct comparison between the City of Norton and Town of Lebanon.

It should be noted that Norton had missing data during every cold season from 1990-1998 before a larger 8"-diameter NWS rain gage was installed at the Water Plant.  By contrast, the entire data period of Lebanon was recorded with a 8"-diameter NWS gauge.

Similar comparisons between Norton & Richlands find somewhat greater differences in favor of much more annual precipitation in Norton.

Northeast of Lebanon and Richlands annual amounts decrease further into locations such as Tazewell, Bluefield, and Bland ( in the mean ).  Burkes Garden has somewhat more ( but reference remarks below ).

This is not just about moisture extraction 
by the High Knob Landform, since during the convective season many documented cases of shower & thunderstorm formation triggered by clouds developing above the massif are noted to provide rainfall to the Clinch Valley as they drift east to southeast off the massif and Tennessee Valley Divide into Russell & Scott counties.

In addition, large amounts of secondary moisture via fog drip from trees and vegetation are added to the Clinch Valley as cold air drains downward out of the highcountry of the massif and Tennessee Valley Divide to often form nocturnal inversions which develop and trap a dense fog layer within the corridor from The Pinnacle Natural Area Preserve southwest to the Rye Cove Karst Basin ( near Natural Tunnel State Park ).

But long-term differences are simply amazing as exemplified by Burkes Garden sitting upon the Tennessee Valley Divide at the head of the Clinch River Basin, where despite its high elevation and long record period ( 1896-Present ) there has been only 1 year ( January-December period ) with more than 60" of total precipitation ( 63.02" in 1972 ).

*While Big Cherry Dam and Burkes Garden measuring sites are close to the same elevation, Big Cherry Dam has averaged 23.98" more per year than Burkes Garden during the 2009-2011 period ( despite the significant precipitation losses at Big Cherry Dam ).

*As of November 2011.



Biodiversity Enhanced 
By Climate Over Time Working 
Upon A Complex Landform

High Knob Lake Basin
Yellow Coral Mushroom Species
Photograph by Roddy Addington - © All Rights Reserved.

While the variation in 2011 precipitation amounts shown above for Virginia is but a single example of a single year, it tends to define the main zone of Mixed Mesophytes where the most mesic species live, as first designated by Lucy Braun, eastward of which reside communities dominated by Oaks 
( Quercus spp. ) and species of the Pinaceae Family.

However, as Braun detailed in her premier book Deciduous Forests Of Eastern North America, nothing in the natural world is ever so simple such that much ecological work in the decades since her research has focused upon identification of many natural communities within these major forest zones which are dictated by climate and terrain.

Braun observed this in the Cumberland Mountains where changes in altitude, geology, and climate all worked together to determine what species lived where amid the larger-scale domain of its diverse Mixed Mesophytic Forests.

It should also be pointed out that in the decades since Lucy & Annette walked amid Appalachian forests there have been many changes, some anthropogenic and others related to replacement of species like the great American Chestnut ( Castanea dentata ).

Numerous studies suggesting a trend toward more mesic, shade tolerant species replacement of more xeric, shade intolerant species over time
( e.g., maples replacing oaks in natural settings undisturbed by man ).

Jefferson National Forest
High Knob Lake Special Biological Area
Unidentified Mushroom Species - High Knob Lake Basin
Photograph by Roddy Addington - © All Rights Reserved.

The more I study the High Knob Landform the more complex it is found to become, with a vast array of micro-climatologic variations that act to complicate & expand its diversity for both surface and subterranean life forms ( including humans ).

The calcareous core that breaches the High Knob Landform, even extending inside of its massif, is a notable complication as it also acts to breach the Mixed Mesophytic Forest domain with settings suitable for many new and different species not typically found with mixed mesophytes ( wetness in this area making it distinct from the much drier calcareous landscapes to the east and northeast of the High Knob Landform ).

While soil types and their porosity are very important factors, total precipitation and its frequency, fog, rime, cloudiness, and temperatures are also vital to types of species observed at any given elevation and exposure.

High Knob Lake Basin of High Knob Massif
Colorful Mushroom Growing In Abundant Wetness
Photograph by Roddy Addington - © All Rights Reserved.

An example of the above can be given by listing a few of the natural communities which have been identified within the High Knob Landform.


Natural Communities Of
*The High Knob Landform

Southern Appalachian Northern Hardwoods
( Upper elevations of High Knob Massif )

High Elevation Cove Forests
( e.g., High Knob Lake Basin )

Mixed Mesophytic Northern Hardwoods
( Cold air drainage corridors of massif )

Rich Cove-Slope Forest
( Exemplifies Mixed Mesophytic Forest )

Canadian Hemlock Forest
( Endangered by Adelges tsugae )

Acidic Cove Forest
( Mesic but more infertile mountain slopes )

Mountain Acidic Woodland
( Edaphically stressed, oligotrophic soils )

Mountain Acidic Cliff
( e.g., precipitous quartz-arenite sandstones )

High Knob Massif
Pickem-Little Stone Mountains
Xeric Sandstone Cliff Communities
Photograph by Tom Rawinski - © VANHP All Rights Reserved.
( Virginia Natural Heritage Program )

Mountain Acidic Seepage Swamp
( e.g., Glady Fork Basin )

Oak-Heath Forest
( Xeric, infertile upland sites )

Pine-Oak / Heath Forest
( Rocky, convex ridges and cliff tops )

Montane Mixed Oak / Oak-Hickory Forest

Low-elevation Acidic Outcrop Barren

Mountain Basic Woodland

Mountain Calcareous Cliff
( e.g., Great Belt of Greenbrier Limestone Cliffs )

Calcareous Fen / Seep

Dry-mesic Calcareous Forest

Montane Dry Calcareous Forest

Limestone-Dolomite Barren
( e.g., The Cedars )

Low-elevation Basic Outcrop Barren

Low-elevation Boulderfield Forest
( e.g., Rocky Hollow & Back Stone Mountain )

Low-elevation Alluvial Forest
( e.g., Hanging Rock, Ka )

Spray Cliff
( e.g., Little Stony Basin )

Appalachian Bog
( e.g., Laurel Fork Basin )

Mountain Sinkhole Pond
( e.g., Back Stone Mountain )

Semipermanent Impoundments
( e.g., lakes & beaver or man-made ponds )

Appalachian Cave Stream Community

Appalachian Terrestrial Riparian Cave Community

Appalachian Edaphobitic / 
Epikarstic Terrestrial Cave Community

Appalachian Terrestrial Dung / 
Transitory Organic Matter Cave Community

*Many natural communities have been recognized by field work of the Virginia Natural Heritage Program .  Others have been classified based upon local research.  Many more likely exist.

Reference this main section:
The High Knob Landform


Example of: 
A Natural Community
Corridor In The High Knob Massif

High Knob Lake Basin
High Elevation Cove Forest Ecosystem
Photograph by Roddy Addington - © All Rights Reserved.

Due to the unique geology of the remnant massif of highcountry surrounding the peak of High Knob there is today an array of lofty basins and drainages that plunge through steep gorges, creating elevated cold air collection pockets which eventually drain their contents into lower terrain.

These cold air drainages carry more than just air, and over time have created interesting and also important micro-climates supportive of the downward migration of numerous species with northern affinities into elevation ranges where 
they are not typically expected to live.

Mixed Mesophytic Northern Hardwoods are what I find to be the best designation for many of these cold air drainage corridors since conditions tend to be very mesic and cool throughout the year, with distinct northern species mixed into the various natural communities through which they traverse ( climatic wetness highly favoring mesic species ).

The ultimate result being formation of new natural communities themselves, ones that finger down from upper elevations where northern species are more widespread to form mixed composition zones distinct from many of the communities adjoining their descent into lower elevations.

Jefferson National Forest
Fungi Species of High Knob Lake Basin
Photograph by Roddy Addington - © All Rights Reserved.


A Few Representative Species
Mixed Mesophytic Northern Hardwoods
( Cold Air Drainage Corridors of High Knob Massif )

Sugar Maple 
( Acer saccharum var. saccharum )

American Basswood 
( Tilia americana var. americana )

Fraser Magnolia 
( Magnolia fraseri )

Yellow Birch 
( Betula alleghaniensis )

Canadian Hemlock
( Tsuga canadensis )

American Beech 
( Fagus grandifolia )

Striped Maple 
( Acer pensylvanicum )

Mountain Maple 
( Acer spicatum )

Hobble Bush 
( Viburnum lantanoides )

Northern Wild Rasin 
( Viburnum cassinoides )

Rosebay Rhododendron
( Rhododendron maximum )

Mountain Wood Sorrel 
( Oxalis acetosella )

Sweet White Violet 
( Viola blanda var. blanda )

Canada Violet
( Viola canadensis var. canadensis )

Red Elderberry
( Sambucus racemosa var. pubens )

Painted Trillium 
( Trillium undulatum )

Furrowed Wake Robin 
( Trillium sulcatum )

Canada Mayflower
( Maianthemum canadense )

Showy Orchis 
( Galearis spectabilis )

Appalachian or Small's Twayblade Orchid
( Listera smallii )

Yellow Mandarin
( Prosartes lanuginosa )

Maple-leaved Waterleaf 
( Hydrophyllum canadense )

Species compositions of Mixed Mesophytic Northern Hardwood corridors are naturally variable, with those drainages possessing northern & eastern exposures as well as those draining major cold air basins tending to have the most northern species.

There are many more natural communities across the great High Knob Landform which have not been listed or even yet identified, both above and beneath  its surfaces!